42 Clare Dennis Avenue
42 Clare Dennis Avenue, Gordon ACT 2906, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Jun 1991 | $136,950 | $160 |
| Sold | Nov 1990 | $36,000 | $42 |
Price per m² based on land size of 854 m².
Key details
- Locality
- Gordon
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714854836
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/GORD/461/7
- Remoteness area
- Metro
- Property type
- House
- Land size
- 854 m²
- Internal area
- -
- Land Use Category
What the land is mainly used for, such as Residential, Commercial, Industrial or Other.
- Residential
Real Estate Agencies
Nearby schools
Frequently asked questions
What is the size of the land for 42 Clare Dennis Avenue?
The property sits on a block measuring 854 m². It offers ample space for a garden, outdoor entertaining or future extensions.
What type of dwelling is located at 42 Clare Dennis Avenue?
The address is a detached house. It is a standalone residence typical of the Gordon neighbourhood.
In which suburb and postcode is 42 Clare Dennis Avenue located?
The property is situated in Gordon, a suburb of Canberra in the Australian Capital Territory, with the postcode 2906.
What natural parks or water features are close to the property?
Point Hut Pond and its district park lie within Gordon itself. Within a 2–3 km radius you’ll also find Gordonvale Park, Pine Island Reserve and Stranger Pond.
Which hills or elevated landmarks are near 42 Clare Dennis Avenue?
Barneys Hill is about 1 km to the north, and Tuggeranong Hill lies roughly 2 km away, providing nearby natural viewpoints.
How far is the property from neighboring suburbs such as Bonython and Conder?
Bonython and Conder are each around 1.5–2 km from the house, making local amenities and services easily reachable.
What geological features are found in the Gordon area?
The southern and central parts of Gordon contain Quaternary alluvium deposits, while the northern section is underlain by Silurian‑age Deakin Volcanics rhyodacitic crystal tuff.